421 resultados para Ramón Menéndez Pidal


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El director de personal d'una empresa va rebre un informe en que se li suggeria que un important problema de formació podria ser resolt amb l'ajut d'un sistema TEL. Es va plantajar el tema en una reunió de l'equip directiu, pero cap deis assistents no tenia una noció precisa del que significava aixo. Al director de formació li encarregaren d'estudiar la qüestió. Afortunadament, aquells dies se celebraven en una ciutat europea una conferencia i una exhibició sobre TEL, i va decidir d'anar-hi. Després de visitar molts stands, assistir a demostracions i establir diversos contactes, tingué la impressió que era més rellevant la qualitat deis grafics que no pas el contingut de formació; molts deis paquets d'EA0 no eran sinó reculls d'exercicis i molt rarament semblava que s'hi haguessin tingut en compte els principis d'aprenentatge més elementals.

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M'han sol-licitat una breu presentació del treball que realitzem al grup 1 més 0, que jo coordino. Tractaré de resumir-ne les línies d'investigació en la brevetat de l'espai que m'han destinat. Com que el treball que es presenta és obra de diverses persones, hem inclas les seves adreces electròniques com a referéncies.

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Major coastal storms, associated with strong winds, high waves and intensified currents, and occasionally with heavy rains and flash floods, are mostly known because of the serious damage they can cause along the shoreline and the threats they pose to navigation. However, there is a profound lack of knowledge on the deep-sea impacts of severe coastal storms. Concurrent measurements of key parameters along the coast and in the deep-sea are extremely rare. Here we present a unique data set showing how one of the most extreme coastal storms of the last decades lashing the Western Mediterranean Sea rapidly impacted the deep-sea ecosystem. The storm peaked the 26th of December 2008 leading to the remobilization of a shallow-water reservoir of marine organic carbon associated with fine particles and resulting in its redistribution across the deep basin. The storm also initiated the movement of large amounts of coarse shelf sediment, which abraded and buried benthic communities. Our findings demonstrate, first, that severe coastal storms are highly efficient in transporting organic carbon from shallow water to deep water, thus contributing to its sequestration and, second, that natural, intermittent atmospheric drivers sensitive to global climate change have the potential to tremendously impact the largest and least known ecosystem on Earth, the deep-sea ecosystem.

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Evergreen Nothofagus betuloides and decidoues N. pumilo form the main forest types in Tierra del Fuego. These forest were sampled along two altitudinal gradients to study their structure and dynamics and assess the causes of their distribution.

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Gammarus aequicauda and Sphaeroma hookeri are the most abundant macroinvertebrates on Ruppia cirrhosa (1275 and 1290 individuals.m-2) and Potamogeton pectinatus (140 and 680 individuals. m-2) in Tancada lagoon, a Mediterranean coastal lagoon in the Ebro Delta (NE Spain). Consumption and assimilation efficiencies were calculated from bell jar experiments. Gammarus grazing effects are higher than Sphaeroma on both Ruppia cirrhosa and Potamogeton pectinatus. Green Ruppia leaves lost 0.3 mg per mg Gammarus per day, while Potamogeton leaves lost 0.2 mg per mg Gammarus per day. Decomposing Ruppia leaves lost 0.35-0.54 mg per mg Gammarus per day. Losses of weight by both Ruppia and Potamogeton due to Sphaeroma feeding were less than half those by Gammarus. Assimilation efficiencies are higher for Gammarus (44-78% feeding on Ruppia 2% feeding on Potamogeton) than for Sphaeroma (26-48%) feeding on Ruppia). These assimilation efficiencies were higher than those reported by other authors working at higher latitudes perhaps because of the higher temperature under which the experiments were carried out.

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Coastal lagoons where salinity varies within a wide range during the year are colonized by euryhaline macrophytes which can develop extensive beds. Seasonal changes in biomass of Ruppia cirrhosa and Potamogeton pectinatus were studied in Tancada Lagoon (Ebro Delta, NE Spain) in order to reveal the environmental factors controlling their population development. Ruppia cirrhosa occupy a larger area of the lagoon than Potarnogeton pectinatus. Their maximum above ground biomasses are also different (495 g m-2 and 351 g m-2 ash free dry weight, respectively). Below ground biomass of Ruppia cirrhosa is between 9 and 53 % of the above ground biomass, while it is 3-40 % for Potamogeton pectinatus. Chlorophyll a contents show fluctuations similar to biomass. Low salinity and high turbidity caused by freshwater inflows favour Potamogeton expansion, while Ruppia development is favoured by high salinity and transparent water.

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The decomposition process of Ruppia cirrhosa was studied in a Mediterranean coastal lagoon in the Delta of the River Ebro (NE Spain). Leaves and shoots of Ruppia were enclosed in 1 mm-mesh and 100 pm-mesh litter bags to ascertain the effect of detritivores, macroinvertebrates, and bacteria and fungi, respectively. Changes in biomass and carbon, and, nitrogen and phosphorus concentrations in the detritus were studied at the sediment-water interface and in the sediment. Significant differences in biomass decay were observed between the two bag types. Significant differences in decomposition were observed between the two experimental conditions studied using 100 pm-mesh bags. These differences were not significant when using the 1 mm-mesh bags. The carbon content in the detritus remained constant during the decomposition process. The percentage of nitrogen increased progressively from an initial 2.4 % to 3 %. The percentage of phosphorus decreased rapidly during the first two days of decomposition from an initial 0.26 % to 0.17 %. This loss is greater in the sediment than in the water column or at the sediment-water interface. From these results we deduce that the activity of microorganisms seems to be more important in the sediment than in the water-sediment interface, and that grazing by macroinvertebrates has less importance in the sediment than in the water column.

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This work aims to characterise the current autotrophic compartment of the Albufera des Grau coastal lagoon (Menorca, Balearic Islands) and to assess the relationship between the submerged macrophytes and the limnological parameters of the lagoon. During the study period the submerged vegetation was dominated by the macrophyte Ruppia cirrhosa, which formed dense extensive meadows covering 79% of the surface. Another macrophyte species, Potamogeton pectinatus, was also observed but only forming small stands near the rushing streams. Macroalgae were only occasionally observed. Macrophyte biomass showed a clear seasonal trend, with maximum values in July. The biomass of R. cirrhosa achieved 1760 g DW m-2, the highest biomass ever reported for this species in the literature. The seasonal production-decomposition cycle of the macrophyte meadows appears to drive the nutrient dynamics and carbon fluxes in the lagoon. Despite the significant biomass accumulation and the absence of a washout of nutrients and organic matter to the sea, the lagoon did not experience a dystrophic collapse. These results indicate that internal metabolism is more important than exchange processes in the lagoon.

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El objeto de nuestro trabajo es el estudio del micromodelado desarrollado sobre granito y su evolución postglacial en dos áreas de los Pirineos Españoles: Panticosa (valle del río Gállego) y Cavallers (valle del río Koguera de Tor). Ambas áreas presentan un modelado principalmente glacial con micro y macro-formas típicas, heredadas de la Última glaciación...

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La alterancia de niveles arcillosos rojizos y limos amarillentos mas o menos encostrados por CaC03, constituyen uno de 10s elementos más tipicos del glacis del Pla de Barcelona. Esta secuencia ha recibido hasta la fecha distintas interpretaciones sobre su origen basadas en criterios de campo y/o diferencias en sus minerales pesados: los niveles rojos y limos amarillos subyacentes son considerados verdaderos suelos diferenciados in situ por unos autores, mientras que son considerados como depósitos de diferente origen por otros autores

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Evergreen Nothofagus betuloides and decidoues N. pumilo form the main forest types in Tierra del Fuego. These forest were sampled along two altitudinal gradients to study their structure and dynamics and assess the causes of their distribution.

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En aquest article es revisen els components de la fertilitat dels sòls mediterramis i es discuteix les seves característiques generals, així com la suposada oligotrofia que sovint se'ls ha atribuït. La tipologia d'aquests sòls i els cicles del N i P presenten alguns trets comuns que vénen determinats per trobar-se en n règim de clima mediterrani, tanmateix existeixen diferències remarcables que es relacionen, sobretot, amb el tipus de roca mare i que expliquen les diferències sovint atribuïdes als sòls de les cinc regions mediterrànies

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Se estudian mineralógicamente los fosfatos miocénicos de Bellver de la Cerdanya (Lérida). Para ello, se emplean las técnicas siguientes: difracción de rayos X, espectroscopia de emisión y absorción de infrarrojos. Mediante el estudio roentgenológico determinamos que la especie mineral en estudio es la Anapaita (FeCaz(P04)2.4Hz0). La espectroscopia de emisión confirma, por una parte, la existencia de los elementos constituyentes de la fórmula química: P, Ca y Fe con líneas bien marcadas y, por otra parte, la presencia de Mn, Al, Si, Mg, Na y Cu como contaminantes. Finalmente, el estudio del espectro de absorción de rayos infrarrojos detecta el grupo fosfato, básico, y la presencia de agua de absorción.

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Evergreen Nothofagus betuloides and decidoues N. pumilo form the main forest types in Tierra del Fuego. These forest were sampled along two altitudinal gradients to study their structure and dynamics and assess the causes of their distribution.

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Se estudian cuatro comunidades ruderales de los alrededores de Barcelona (Chenopodietum muralis, Silybo-Urticetum, Carduo-Hordeetum eInulo-Oryzopsietum) desde una perspectiva fitosociológica (inventarios florísticos, espectros de familias, distribución fitogeografica y formas vitales) y edafológica (analisis de parametros físico-químicos del suelo, con especial énfasis en las formas minerales de nitrogeno). Los resultados ponen de manifiesto la variabilidad de hábitats y composición florística de estas comunidades. Por otra parte, las bajas acumulaciones de diferentes formas de N mineral no parecen confirmar su pretendida nitrofilia.